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Kleiner Solstein
The Kleiner Solstein is a mountain, high, in the Nordkette in the Karwendel Alps in the Austrian state of Tyrol. Despite its name ("Small Solstein") it towers above its western neighbour, the Großer Solstein ("Great Solstein") () by almost and is thus the highest summit in the Nordkette. The southern side of the Kleiner Solstein facing the Inn valley is characterised by ''schrofen'' and steep-sided cirques. To the north it plummets in a rock face up to high towards the valley of ''Großkristental'', which runs from the Gleirsch valley in a southwesterly direction to the Erl Saddle. Ascent The normal route to the Kleiner Solstein runs from the saddle between the Großer and Kleiner Solstein, initially crossing a small ridge of rock (''Felsrippe'') then over ''schrofen'' from the south to the flat summit ridge following a waymarked route to the top. The route to the saddle between the two peaks may be reached either from the Solsteinhaus and the Großer Solstein or on two ...
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Hintere Brandjochspitze
The Hintere Brandjochspitze () is a summit roughly 200 metres northwest of the Vordere Brandjochspitze in the Nordkette range above Innsbruck. It rises above its "forward" neighbour by around 40 metres. The summit may be reached in 20 minutes from the Vordere Brandjochspitze at climbing grade UIAA I through a gully left of the arête An arête ( ) is a narrow ridge of rock which separates two valleys. It is typically formed when two glaciers erode parallel U-shaped valleys. Arêtes can also form when two glacial cirques erode headwards towards one another, although frequen .... A more difficult route runs along the western arête (grade III-) from the Hohe Warte. Other routes along the northern ''Hippengrat'' ( UIAA IV) from the ''Hippenspitze'' (2,388 m) and from the northwest ( UIAA IV) are rarely used. Literature * (Hippengrat, northwest route) * (normal route, west arête) {{authority control Two-thousanders of Austria Karwendel Mountai ...
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Cirque
A (; from the Latin word ') is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are corrie (from Scottish Gaelic , meaning a pot or cauldron) and (; ). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped, as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens. Hence, it experiences somewhat greater erosion forces and is most often overdeepened below the level of the cirque's low-side outlet (stage) and its down-slope (backstage) valley. If the cirque is subject to seasonal melting, the floor of the cirque most often forms a tarn (small lake) behind a dam, which marks the down ...
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Mountains Of Tyrol (state)
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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Two-thousanders Of Austria
Two-thousanders are mountains that have a height of at least 2,000 metres above sea level, but less than 3,000 metres. The term is used in Alpine circles, especially in Europe (e.g. German: ''Zweitausender''). The two photographs show two typical two-thousanders in the Alps that illustrate different types of mountain. The Säuling (top) is a prominent, individual peak, whereas the Schneeberg (bottom) is an elongated limestone massif. In ranges like the Allgäu Alps, the Gesäuse or the Styrian-Lower Austrian Limestone Alps the mountain tour descriptions for mountaineers or hikers commonly include the two-thousanders, especially in areas where only a few summits exceed this level. Examples from these regions of the Eastern Alps are: * the striking Nebelhorn (2,224 m) near Oberstdorf or the Säuling (2,047 m) near Neuschwanstein, * the Admonter Reichenstein (2,251 m), Eisenerzer Reichenstein (2,165 m), Großer Pyhrgas (2,244 m) or Hochtor (2,369&nbs ...
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Alpenvereinsführer
The ''Alpine Club Guides'' (german: Alpenvereinsführer, commonly shortened to ''AV Führer'' or ''AVF'') are the standard series of Alpine guides that cover all the important mountain groups in the Eastern Alps. They are produced jointly by the German (DAV), Austrian (ÖAV) and South Tyrol Alpine Clubs (AVS). They have been published since 1950 by the firm of Bergverlag Rother in Munich, Germany. The AV guides contain all the routes – hiking trails, mountain hut approaches and summit climbs as well as ice and high mountain routes and ''klettersteigs'' in each mountain range. The descriptions are factual and dry, with few illustrations - rather unlike mountain books by e.g. Walter Pause – and despite introductory sections require general Alpine knowledge and experience. Examples are the ''AVF Allgäuer Alpen'' and the ''AVF Verwallgruppe''.The AV guides are often used as the basis for other publications and complement the Alpine Club maps or other map series. Available guid ...
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Climbing Route
A climbing route is a path by which a climber reaches the top of a mountain, rock, or ice wall. Routes can vary dramatically in difficulty and grade; once committed to that ascent, it can sometimes be difficult to stop or return. Choice of route can be critically important. Guidebooks, if available, are helpful in providing detailed diagrams and photographs of routes. In the earliest days of hillwalking and mountaineering, climbers got to the top by whatever means got them there. Little information about how they did it is available. During the 19th century, as explorers of the Alps tried ever harder summits, it became clear that choosing an eastern face over a southwestern ridge could spell the difference between success or failure. One example was the first ascent of the Matterhorn, which had been repeatedly and unsuccessfully attempted via the southern side. The strata there tended to slope down and away while the rocks of the northeastern ridge (the one closest to Ze ...
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Arête
An arête ( ) is a narrow ridge of rock which separates two valleys. It is typically formed when two glaciers erode parallel U-shaped valleys. Arêtes can also form when two glacial cirques erode headwards towards one another, although frequently this results in a saddle-shaped pass, called a col. The edge is then sharpened by freeze-thaw weathering, and the slope on either side of the arête steepened through mass wasting Mass wasting, also known as mass movement, is a general term for the movement of rock or soil down slopes under the force of gravity. It differs from other processes of erosion in that the debris transported by mass wasting is not entrained in ... events and the erosion of exposed, unstable rock. The word ''arête'' () is actually French for "edge" or "ridge"; similar features in the Alps are often described with the German language, German equivalent term ''Grat''. Where three or more cirques meet, a pyramidal peak is created. Cleaver A ''cleaver' ...
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Climbing Grade
In rock climbing, mountaineering, and other climbing disciplines, climbers give a grade to a climbing route or boulder problem, intended to describe concisely the difficulty and danger of climbing it. Different types of climbing (such as sport climbing, bouldering or ice climbing) each have their own grading systems, and many nationalities developed their own, distinctive grading systems. There are a number of factors that contribute to the difficulty of a climb, including the technical difficulty of the moves, the strength, stamina and level of commitment required, and the difficulty of protecting the climber. Different grading systems consider these factors in different ways, so no two grading systems have an exact one-to-one correspondence. Climbing grades are inherently subjective.Reynolds Sagar, Heather, 2007, ''Climbing your best: training to maximize your performance'', Stackpole Books, UK, 9. They may be the opinion of one or a few climbers, often the first ascensi ...
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Solsteinhaus
The Solsteinhaus is an Alpine Club hut belonging to the Austrian Alpine Club located at a height of on the Erl Saddle (''Erlsattel'') between the mountains of the Nordkette and Erlspitze Group. It was opened in 1914 and totally renovated in 2007. It lies in the western Karwendel Alps in the state of Tyrol not far from the state capital of Innsbruck. Due to its central location and the numerous tour options it offers, the hut is a base for climbers taking part in tours of several days long, as well as a starting point for summit attempts. In addition the hut is a popular destination for hikers who can easily do a day tour to the hut. In winter the hut is closed, but there is a winter room for ski tourers. During safe avalanche conditions, high Alpine ski tours can be undertaken to the surrounding summits; but these all require good experience. Visit of Bruno the Bear / JJ1 In the evening hours of 7 June 2006 a brown bear, JJ1, otherwise known as Bruno, was seen from the Sol ...
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Waymark
Trail blazing or way marking is the practice of marking paths in outdoor recreational areas with signs or markings that follow each other at certain, though not necessarily exactly defined, distances and mark the direction of the trail. A blaze in the beginning meant "a mark made on a tree by slashing the bark" (''The Canadian Oxford Dictionary''). Originally a waymark was "any conspicuous object which serves as a guide to travellers; a landmark" (''Oxford English Dictionary''). There are several ways of marking trails, including paint, carvings, affixed markers, posts, flagging, cairns, and crosses, with paint being the most widely used. Types of signage Paint A painted marking of a consistent shape or shapes (often rectangular), dimension and colour or combination of colours is used along the trail route. The system by which blazes are used to signify turns and endpoints in trails (see below) strongly favors the use of paint blazes. European countries usually use systems ...
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Normal Route
A normal route or normal way (french: voie normale; german: Normalweg) is the most frequently used route for ascending and descending a mountain peak. It is usually the simplest route. Overview In the Alps, routes are classed in the following ways, based on their waymarking, construction and upkeep: * Footpaths (''Fußwege'') *Hiking trails (''Wanderwege'') * Mountain trails (''Bergwege'') * Alpine routes (''Alpine Routen'') *Climbing routes (''Kletterrouten'') and High Alpine routes (''Hochalpine Routen'') in combined rock and ice terrain, (UIAA) graded by difficulty Sometimes the normal route is not the easiest ascent to the summit, but just the one that is most used. There may be technically easier variations. This is especially the case on the Watzmannfrau, the Hochkalter and also Mount Everest. There may be many reasons these easier options are less well-used: * the simplest route is less well known than the normal route (Watzmannfrau). * the technically easiest route is mor ...
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